Cool.I have worked a wee bit with zeolites, mostly some synthetic ones for coating applications.
The pore sizes were desirable and even the cation exchange capacity was of some utility. I've got a patent application in using zeolites in one of our processes.
I looked at a sandstone once that had a zeolite cement. Really strange. The zeolite was low birefringence and formed isopachous rims that grew off of the grains and filled intergranular pores completely. It yielded this weird pseudouniaxial cross in every pore.I have never done any optical microscopy on them, but crystallographically they are waaay cool. At one point I bought one of those inorganic compound model sets and built one of the crystals to show around at meetings when I was pushing these for some of our coating applications.
This is what cemented our rock above! Was produced by alteration of neovolcanic lithic grains, mostly volcanic glass shards.But I always ended up working with this one:
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(Clinoptilolite)
I left my hammer in my carry on one time. I miss that hammer.Just as an FYI: don't try to take these materials through TSA in your hand luggage! Ship it.
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